Foraminiferal response to the PETM recorded in the SW Tarim Basin, central Asia

The Paleocene/Eocene (P/E) boundary interval is the most significant climatic transition during the Cenozoic, when the PETM (Paleocene Eocene Thermal Maximum) caused rapid warming and severe fluctuation of the Earth system, especially in marine settings. The SW Tarim Basin represents a distal branch...

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Published inPalaeogeography, palaeoclimatology, palaeoecology Vol. 506; pp. 217 - 225
Main Authors Jiang, Tian, Wan, Xiaoqiao, Aitchison, Jonathan C., Xi, Dangpeng, Cao, Wenxin
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.10.2018
Subjects
basins
Central Asia
Earth system science
Eocene epoch
Foraminiferal biostratigraphy
marine environment
microfossils
mudstone
Northeastern Tethys
Paleocene epoch
Paleocene/Eocene boundary
plankton
Retaria
sea level
Central Asia
Northeastern Tethys
Foraminiferal biostratigraphy
Paleocene/Eocene boundary
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Summary:The Paleocene/Eocene (P/E) boundary interval is the most significant climatic transition during the Cenozoic, when the PETM (Paleocene Eocene Thermal Maximum) caused rapid warming and severe fluctuation of the Earth system, especially in marine settings. The SW Tarim Basin represents a distal branch of the NE Tethys, exposing Paleocene to Eocene successions that include the Qimugen Formation and provide optimal section for investigating the P/E boundary transition. By detail field-based lithological records and the planktonic and benthic foraminiferal assemblage analysis, the P/E boundary was redefined within the black mudstone bed of the Qimugen Formation. The planktonic foraminiferal assemblages recorded in the Qimugen Formation may be subdivided into four biozones, including bioevents of Globanomalina pseudomenardii, Globanomalina luxorensis and Pseudohastigerina wilcoxensis. Planktonic foraminiferal turnover is marked by the cool water subbotinids disappearance, give way to warm water muricate taxa, co-varying with the gradual disappearance of benthic foraminifera. The foraminiferal assemblages together with other identified microfossils suggest a shallow marine environment in which transgressions related to the sea level fluctuation of the Tethyan Domain took place in the Paleocene to Eocene boundary interval. [Display omitted] •Foraminiferal biostratigraphy of P/E boundary in easternmost Tethys, central Asia•P-E transition marked by planktonic and benthic foraminiferal faunal turnover•Shallow marine palaeoenvironment proposed with transgression from Tethyan Domain
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ISSN:0031-0182
DOI:10.1016/j.palaeo.2018.06.041